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feet, respectively. Because the drawdowns due to pit inflows will be mostly <br /> contained within the leasehold area, and adjacent water users are located <br /> beyond the one foot drawdown contours, no significant impact on <br /> groundwater use due to pit inflows is predicted. <br /> Impacts of Production Well <br /> Seneca Coal Company predicted that maximum drawdowns in the Trout <br /> Creek aquifer resulting from nine years of pumping in the Yeast Production <br /> Well would be 186 feet. After 20 years of recovery, the residual drawdown <br /> within one mile of the well is predicted to be less than two feet. The radial <br /> distance to the one foot drawdown contour after 20 years of pumping was <br /> predicted to be 10 miles. The only known Trout Creek wells within this <br /> radius are associated with the Twentymile Coal Mine and are between seven <br /> and ten mile from the proposed Yeast Mine well. The drawdown at this <br /> distance from the Yeast Mine well should not significantly impact these <br /> wells. <br /> Streamflow depletions in the Yampa River, Fish Creek, Middle Creek and <br /> Trout Creek channels due to changes in the groundwater regime were all <br /> predicted to be less than 0.55 acre-feet per year. However, streamflow <br /> depletions in Sage Creek and Grassy Creek were predicted to be higher: 4.9 <br /> acre-feet per year in Sage Creek and 5.8 acre-feet per year in Grassy Creek. <br /> Impact of Replaced•Spoil on Groundwater <br /> Seneca Coal Company predicted that the replaced spoil would have a 25% <br /> higher hydraulic conductivity than the undisturbed material. Other than that, <br /> the primary effect on groundwater would be degradation of quality with <br /> respect to total dissolved solids (TDS). <br /> Seneca Coal Company predicted that the increase in TDS concentrations in <br /> the bedrock aquifers will range from 70% in the Wadge Overburden to over <br /> 300% in the Wadge Coal. These predictions are for groundwater in close <br /> proximity to the resaturated spoil, within the permit area. As groundwater <br /> migrates away from the resaturated spoil, mixing, dilution from unaffected <br /> recharge, and geochemical changes will decrease the TDS concentrations. <br /> Well yields in these bedrock units, the Wadge Coal and Overburden and the <br /> Wolf Creek Coal and Overburden, are insufficient for irrigation purposes. <br /> The alluvial aquifers that will be affected by the resaturated spoil include the <br /> Annand Draw, Upper Grassy Creek, Lower Grassy Creek, and Sage Creek <br /> alluvium. Within the Grassy Creek basin, above the confluence with <br /> Scotchman's Gulch, the magnitude of the TDS increase will be high <br /> immediately below the resaturated spoil, but will be undetectable a short <br /> Yoast Mine 25 October 19, 1999 <br />